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Sorption of Molybdates and Tungstates on Functionalized Montmorillonites: Structural and Textural Features

机译:钼酸盐和钨酸盐在功能化蒙脱石上的吸附:结构和结构特征

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摘要

Montmorillonite—the most popular mineral of the smectite group—has been recognized as a low-cost, easily available mineral sorbent of heavy metals and other organic and inorganic compounds that pollute water. The aim of this work was to determine the sorption mechanism and to identify the reaction products formed on the surface of montmorillonite and organo-montmorillonite after sorption of molybdates (Mo(VI)) and tungstates (W(VI)). Montmorillonites are often modified to generate a negative charge on the surface. The main objective of the study was to investigate and compare the features of Na-montmorillonite (Na-M), montmorillonite modified with dodecyl trimethyl ammonium bromide (DDTMA-M), and montmorillonite modified with didodecyl dimethyl ammonium bromide (DDDDMA-M) before and after sorption experiments. The material obtained after sorption was studied by X-ray diffraction (XRD), Fourier-transform infrared spectroscopy (FTIR), scanning electron microscopy (SEM), and X-ray photoelectron spectroscopy (XPS). The XRD pattern showed the presence of a new crystallic phase in the sample that was observed under an SEM as an accumulation of crystals. The FTIR spectra showed bands related to Mo–O and W–O vibration (840 and 940 cm−1, respectively). The obtained results suggest that molybdenum(VI) and tungsten(VI) ions sorb onto the organo-montmorillonite in the form of alkylammonium molybdates and tungstates.
机译:蒙脱石(蒙脱石族中最受欢迎的矿物)被公认为是低成本,易得的重金属以及污染水的其他有机和无机化合物的矿物吸附剂。这项工作的目的是确定吸附机理,并确定吸附钼酸盐(Mo(VI))和钨酸盐(W(VI))后在蒙脱石和有机蒙脱石表面形成的反应产物。蒙脱土经常被改性以在表面上产生负电荷。本研究的主要目的是研究和比较Na-蒙脱土(Na-M),十二烷基三甲基溴化铵(DDTMA-M)改性的蒙脱土和十二烷基二甲基溴化铵(DDDDMA-M)改性的蒙脱土的特性并经过吸附实验。通过X射线衍射(XRD),傅立叶变换红外光谱(FTIR),扫描电子显微镜(SEM)和X射线光电子能谱(XPS)研究吸附后获得的材料。 XRD图谱显示样品中存在新的结晶相,在SEM下观察到该结晶相是晶体的积累。 FTIR光谱显示出与Mo–O和W–O振动相关的谱带(分别为840 cm和940 cm -1 )。获得的结果表明,钼(VI)和钨(VI)离子以烷基钼酸铵和钨酸盐的形式吸附到有机蒙脱土上。

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